The Everglades Pseudoatoll (also called a pseudo-atoll) was a major geomorphic feature of southern Florida during the Pliocene epoch. Origin The Everglades Pseudoatoll began its growth during the early Eocene as a paleodepression possibly created by an asteroid impact upon the carbonate Florida Platform at the southern part of what is now Everglades National Park. The pseudo-atoll is surrounded by a raised rim. Its growth as a reef system and pseudo-atoll began during the Oligocene reaching its maximum size of north to south during the Piacenzian of the late Pliocene. (Petuch, 163). Description The Everglades Pseudoatoll was a U-shaped asymmetrical system of reefs that surrounded the Okeechobean Sea, not unlike South Pacific atolls surrounded by a central lagoon. The west side was more developed than the east and south, as was the remainder of the west side. On the western side of this pseudo-atoll lay the Immokalee Reef Tract and chain of islands called the Immokalee Archipelago. The large Hendry Platform lay behind the reef on the east. Mangrove forests extended southwesterly of the pseudo-atoll along what would be the southwestern Florida coast. To the northwest was the Myakka Lagoon System, a tropical estuary of brackish water. On the east the lay the Miami-Palm Beach Reef Tract with narrow back reef. Between the west and east was the wide and very deep 100-meter (330 ft) lagoon known as the Loxahatchee Trough. The northern part of the pseudo-atoll was the Kissimmee Embayment which was lined with mud flats and jungles of mangrove. Chronology The pseudo-atoll's chronology is developed from deposition of a variety of community organisms. The oldest are the early Piacenzian communities of shallow intertidal muddy-sand Mercenaria tridacnoides community of clam species, the deep lagoon Nodipecten peedeensis community of scallops, the shallow lagoon Apicula buckinghamensis community of tower shell snails, and lagoon coral Phyllangia blakei community. The second time period is mid-Piacenzian and contains the shallow muddy intertidal Strombus floridanus (conch) communities, shallow lagoon tower shell snail Apicula gladeensis community, lagoon scallop Nodipecten floridensis community, and the shallow lagoon Hyotissa meridionalis community of foam oysters. The third time period is the late Piacenzian and contained wave-action related coral zones of open ocean to sheltered basin. The communities are the high energy open ocean Pocillopora crassoramosa community of the coral reef crest. The back reef Dichocoenia tuberosa community of coral, the low energy back reef Isophyllia desotonsis community of coral, the